Persistent Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Possible
- Taille
- 1.5–3
This layer has been most reactive around treeline, particularly in areas that have not seen significant skier traffic.
Accumulating storm snow is building into a surface slab, which could step down to the lingering persistent slabs.
Less visited areas in Glacier National Park may have more sensitive persistent weak layers, due to less skier/rider traffic cutting up the slabs.
This layer has been most reactive around treeline, particularly in areas that have not seen significant skier traffic.
Low density storm snow, accompanied by moderate ridge-top winds, is forming soft slabs on variable wind-affected surfaces. Sensitivity to triggering will increase with wind spikes throughout the day.
Recently, a large cornice-triggered natural avalanche stepped down to this basal layer. Watch for steep, thin rocky areas where this layer could be activated.
Isolated sz 2 natural avalanches were detected from Smart Peak, Mannix, and MacD Gully 6 overnight.
Several human-triggered sz 1-1.5 avalanches were reported over the weekend on Avalanche Crest, Hermit Slide path, and Swiss Couloir.
A natural cornice failure triggered a size 3 deep persistent slab on the SE slope of Grizzly Peak on Saturday.
15-20cm of storm snow sits atop old wind-affected surfaces in the alpine and treeline.
The early Jan surface hoar is buried 40-70cm and is most prevalent at treeline. The November 17th facet weakness can still be found near the base of the snowpack in many areas.
Continuing flurries with moderate/strong winds aloft and a gradual warming to seasonal norms.
Wed: cloudy, flurries, 5cm snow, Alp high -9*C, light/moderate SW winds
Thurs: mix of sun and cloud, isolated flurries, Alp high -7*C, light/moderate SW winds